THE COLOR OF MINERALS

Importance

Mineral identification

Main qualitative characteristic

Gems

Semi precious stones

provides information

Crystallochemical characteristics

Genetics of minerals

Caused by radioactivity

natural ionizing radiation

formation of color centers of electron holes

halite

halite

fluorite

fluorite

Quartz

Quartz

calcite

calcite

Associated with transition metal ions

Emerald

Emerald

Ruby

Ruby

Rubelite

Rubelite

Rhodonite

Rhodonite

Chrysolite

Chrysolite

Metallic and covalent compounds

Native metals, sulfides and their analogues

Optical Interzonal Electron Transfers and Related Reflection Maxima

Metallic shades (Pyrite)

Metallic shades (Pyrite)

Metallic shades (Gold)

Metallic shades (Gold)

Fundamental absorption band

cinnabar

cinnabar

orpiment

orpiment

cuprite

cuprite

Distinction

Color of minerals

In individual crystals and mineral chunks

In thin sections

Transparent

In polished sections

In reflected light

Color of a mineral

streak

To describe the color

Comparative evaluation

with the color of some commonly known object or substance

Indigo blue

Indigo blue

Green apple

Green apple

Lemon yellow

Lemon yellow

Blood red

Blood red

with "color standards" of minerals

Vermilion red

Vermilion red

Emerald green

Emerald green

colors of metals or alloys

Tin white (Arsenopyrite)

Tin white (Arsenopyrite)

Steel gray (molybdenite)

Steel gray (molybdenite)

Brass yellow (chalcopyrite)

Brass yellow (chalcopyrite)

Copper red (native copper)

Copper red (native copper)

Methods continue to be developed

Three main groups

Idiochromic Minerals

Own color

Constant and predictable component

Blue azurite

Blue azurite

red cinnabar

red cinnabar

malachite green

malachite green

Allochromatic Minerals

Other colors

Variable and unpredictable property

blue on Amazonite (orthoclase)

blue on Amazonite (orthoclase)

yellow in Heliodor (spodumene)

yellow in Heliodor (spodumene)

Rose on quartz

Rose on quartz

Impurities

Pseudochromatic Minerals

False colors

Variable color and unique mineral property

Precious opal

Precious opal

bright reflections of labradorite

bright reflections of labradorite

between

Under the microscope

Impurities in the crystal lattice

Name: Karen Dayanna Molina Rincón
Class Name: Mineralogy and Crystallography

Mineral fine powder color

Another type of idiochromic mineral

electron transfers between different ions

trivalent iron ores

It is produced

When light is transmitted through a mineral

If it does not absorb any length

The mineral is colorless

Chromophores

Main chromophore elements

chromium (Cr)

chromium (Cr)

iron (Fe)

iron (Fe)

manganese (Mn)

manganese (Mn)

titanium (Ti)

titanium (Ti)

cobalt (Co)

cobalt (Co)

copper (Cu)

copper (Cu)

depend on the position they occupy in the crystalline structure of each mineral

Through

dark and purple

yellow and smoky